江汉平原主要河流沉积物磁学特征及其与物源区表壳岩性的响应

张玉芬; 李长安; 康春国; 严玲琴; 邵磊; 张勇

doi:10.3799/dqkx.2011.079

Volume 36 Issue 4

Jul. 2011

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Article Navigation > Earth Science > 2011 > 36(4): 771-778

ZHANG Yu-fen, LI Chang-an, KANG Chun-guo, YAN Ling-qin, SHAO Lei, ZHANG Yong, 2011. Magnetic Characteristics of River Sediments in Jianghan Plain and Response to Rock Types of the Provenance. Earth Science, 36(4): 771-778. doi: 10.3799/dqkx.2011.079

Citation:

ZHANG Yu-fen, LI Chang-an, KANG Chun-guo, YAN Ling-qin, SHAO Lei, ZHANG Yong, 2011. Magnetic Characteristics of River Sediments in Jianghan Plain and Response to Rock Types of the Provenance. Earth Science, 36(4): 771-778. doi: 10.3799/dqkx.2011.079

Citation:

ZHANG Yu-fen, LI Chang-an, KANG Chun-guo, YAN Ling-qin, SHAO Lei, ZHANG Yong, 2011. Magnetic Characteristics of River Sediments in Jianghan Plain and Response to Rock Types of the Provenance. Earth Science, 36(4): 771-778. doi: 10.3799/dqkx.2011.079

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Magnetic Characteristics of River Sediments in Jianghan Plain and Response to Rock Types of the Provenance

doi: 10.3799/dqkx.2011.079

1.
Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2010-09-15
Publish Date: 2011-07-01

Abstract

Abstract

In this paper we report the magnetic characteristics of the confluent river sediments into the Jianghan Plain. Magnetic characteristics are obviously different between different rivers, such as the Yangtze River, Hanjiang River, Zhanghe River, Juhe River, Manaohe River and Qingjiang River, and are well correlated with rock types of the provenance. Magnetic minerals from the Yangtze River and the Hanjiang River are almost ferrimagnetic, which dominate the magnetic characteristics of the samples. Content of ferrimagnetic minerals in the Yangtze River sediments is higher than that in the Hanjiang River. Ferrimagnetic minerals have thicker crystals in the Yangtze River than that in the Hanjiang River, both of which are almost from pseudo-single to multi domain. Higher concentration of ferrimagnetic minerals and thicker magnetic particles are found in the Hanjiang River than the other tributaries of the Yangtze River flowing to Jianghan plain. High concentration of incomplete anti-ferromagnetism minerals and superparamagnetic particles are found in the Mannaohe River and Zhanghe River sediments respectively. High concentration of incomplete anti-ferromagnetism minerals are found in the Qingjiang River sediments, also with thick magnetic particles. Based on the research we conclude that magnetic characteristics of sediments in Jianghan Plain can provide useful information on constraining sediment provenance.
- sediments,
- magnetic characteristics,
- source tracing,
- geophysics

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References(56)

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Magnetic Characteristics of River Sediments in Jianghan Plain and Response to Rock Types of the Provenance

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